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Combined effect of precipitation and earthquakes on the kinematic
of a slow moving landslideThe case of the Maca landslide, Colca Valley, Peru
Bontemps NoélieLarose EricLacroix Pascal
Taipe EduJara Jorge
Why studying slow moving landslides ?
• displacement of the ground due to the gravity
• One of the major threat in mountainous area
• Kinematic driven by different forcings
rapid landslides (m/s)
slow moving landslides (m/an)
Wegener 2018 2
Zerathe et al. , 2016
Lacroix et al. , 2014
Days since the earthquake
Cu
mu
lati
ve d
isp
lace
men
t(c
m)
Me
anve
loci
ty(c
m)
Dai
ly r
ain
fall
(mm
)
10
20
30
10
30
50
Jan 12 Jan 13 Jan 14
Jan 12 Jan 13 Jan 14
Date
Date
Landslide forcing
0
2
4
6
-2
-40 0 40 80 120
earthquake
Human activitiesRiver
rainfall
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problematic
• To better understand the different mechanisms impacting landslide kinematics in active seismic region where both earthquake and rainfall can combine
Use of in-situ data
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Site of study
Bontemps et al. 2018
• Colca river contributing to erosion of lacustrine deposits
• Precipitation follows a season cycle
• intense seismic activity
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The Maca Landslide monitoring
Zerathe et al., 2016
Recording continuously since the beginning of 2016
MAC 3
MAC 2
MAC 1
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6
Weaver (Phys. Rev. Lett. 2001; Science 2005)
𝑉𝑠 =𝜇
𝜌
In rigidity (𝜇)Increase in density (𝜌)
Vs
Method Ambient noise correlation
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=> Monitoring of tiny changes in the soil properties
Earthquake recorded between 2016 and 2017
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Effective precipitation recorded between 2016 and 2017
GPS measurements
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• Combined effect of precipitation and earthquake observable with GPS
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• Co-seismic drop of the seismic surface wave velocity => decrease of the rigidity
• Long term effect of precipitation following a strong shaking event
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Small magnitude earthquake impact (Ml<4)Distance source –landslide :
Ml 3.9 => 7kmMl 3.6 => 3.5 km
• Keefer (1984) and Keefer and Wilson (1989).
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Small magnitude earthquake impact (Ml<4)
Conclusions
• We can see a combination of earthquake and precipitation from GPS time-series
• acceleration of the landslide following low magnitude earthquakes (Ml<4)
• One possible mechanism at the origin is the damage of the soil that ease the way of precipitation into the ground
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Thank you for your attention
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